We must pay attention to the linear landforms when we determine direction and displacement amount ofstrike-slip fault.
判读走滑断层的变位方向及变位量，需注意地貌面上的线性地物。
2
In the typical geological researches, the attitude of rock formation is characterized by using its strike Angle, dip direction Angle and dip Angle.
在经典的地质研究中，岩层的产状都采用走向角、倾向角和倾角这三种参数进行表征。
3
In Longling fault zone and the area north to it, the directionof maximum compressional stress is near NS or NNW, the stress regime is of strike slip type.